The new air world : $b The science of meteorology simplifiedMoore, Willis L. (Willis Luther)
Science
The new air world : $b The science of meteorology simplified
Moore, Willis L. (Willis Luther)
Meteorology
The cooling effect produced by a draught does not necessarily arise
from the wind being cooler, for it may be actually warmer, but arises
from the rapid evaporation it causes on the surface of the skin.
Vapor of water forms a blanket about the earth and prevents it from
scorching during the day and freezing during the night.
=How to Forecast Weather with Only an Aneroid Barometer.= No one
except an expert observer should use the mercurial barometer. The
aneroid will answer as well for the purpose of forecasting from a
single instrument; it is cheaper and less complicated. First learn
your elevation above sea level; then add to the observed reading of
your instrument .10 for each one hundred feet elevation. Note the
fall or rise and the direction of the wind and with the aid of the
table on page 76 highly satisfactory forecasts may be made by any
intelligent person. Skill will come with practice. Write down your
forecasts each day as you make them and the following day note in
a blank space left for the purpose the success or failure of your
effort. Thus will you profit by your mistakes.
As a rule winds from the east quadrants and falling barometer
indicate foul weather, and winds shifting to the west quadrants
indicate clearing and fair weather. The rapidity of the storm’s
approach and its severity are indicated by the rate and the amount in
the fall of the barometer. This applies to the Mississippi Valley and
eastward to the Atlantic Ocean. Conditions are different in the Rocky
Mountains, on the plateau of the mountains, and on the eastern Rocky
Mountain slope, where precipitation seldom begins until after the
barometer begins to rise after a fall, and the winds have shifted to
the northwest.
Keep in mind that storms are great atmospheric eddies drifting from
the west, with the winds blowing cyclonically toward the center; that
when your wind is northeast the center of the storm is southwest of
you; that when it is east the center is west; when it is south the
center is north; when it is southwest the center is northeast, and
when it is west or northwest the center is east of you.
Public-domain text, read in full here on John Shaqi.
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